GROUNDWATER INVESTIGATION USING GEOPHYSICAL METHODS- A CASE STUDY OF PYDIBHIMAVARAM INDUSTRIAL AREA
|
|
- Drusilla Murphy
- 6 years ago
- Views:
Transcription
1 GROUNDWATER INVESTIGATION USING GEOPHYSICAL METHODS- A CASE STUDY OF PYDIBHIMAVARAM INDUSTRIAL AREA G.VenkataRao 1, P.Kalpana 2, R. Srinivasa Rao 3 1,3 Department of Civil Engineering, GMR Institute of Technology, Andhra Pradesh, India. 2 Department of Chemical Engineering, GMR Institute of Technology, Andhra Pradesh, India. venkatarao.g@gmrit.org Abstract A geophysical investigation involving the vertical electrical sounding (VES) electrical resistivity methods was carried out around Pydibhimavaram Industrial area Srikakulam district Andhra Pradesh. Vertical Electrical Sounding (VES) using Schlumberger array was conducted at thirteen (13) VES stations. The study was carried out with a view to determine the subsurface layer parameters (resistivity s and thicknesses) and use same to categorize the ground-water potential of the study area. The field data obtained have been analyzed using computer software (IPI2win) which gives an automatic interpretation of the apparent resistivity. The interpretation of results showed that major portion of the study area was three layer formations. A vast range of resistivities and their corresponding thicknesses were obtained. Pseudo sections and Geo-electric Sections were generated using Surfer software. The pseudo-sections revealed that the North West (NW) and South West (SW) regions are comparatively more weathered than the other parts. Key words: Vertical Electrical Sounding (VES), Industrial area, resistivity, Soil layers & Geo- electric sections...***... INTRODUCTION Groundwater is a mysterious nature s hidden treasure. Its exploitation has continued to remain an important issue due to its unalloyed needs. Though there are other sources of water; streams, rivers ponds, etc., none is as hygienic as groundwater because groundwater has an excellent natural microbiological quality and generally adequate chemical quality for most uses [1]. The use of geophysics for both groundwater resource mapping and for water quality evaluations has increased dramatically over the years. The Vertical Electrical Soundings (VES) has proved very popular with groundwater studies due to simplicity of the technique. Groundwater has become immensely important for human water supply in urban and rural areas in developed and[2] Exploration of groundwater in hard rock terrain is a very challenging and difficult task when the promising groundwater zones are associated with fractured and fissured media. In this environment, the groundwater potentiality depends mainly on the thickness of the weathered/fractured layer overlying the basement [3]. The use of geophysics for engineering studies and water groundwater exploration has increased over the last few years due to the rapid advances in computer software s and associated numerical modeling solutions. The Vertical Electrical Sounding (VES) has proved very popular with groundwater prospecting and engineering investigations due to simplicity of the techniques. The electrical geophysical survey method is the detection of the surface effects produced by the flow of electric current inside the earth. The electrical techniques have been used in a wide range of geophysical investigations such as mineral exploration, engineering studies, geothermal exploration, archeological investigations, permafrost mapping and geological mapping[4]. Using this method, depth and thickness of various subsurface layers and their water yielding capabilities can be inferred. Therefore, evaluation of groundwater potential at Pydibhimavaram Industrial area was done in order to know the groundwater yielding capabilities or groundwater conditions of the study area. LOCATION AND GEOLOGY OF THE STUDY AREA Location The present study involves delineation of depth of water table and groundwater potential at Pydibheemavaram, a village in Ranastalam mandal in Srikakulam district. It is 28km far from district head quarters Srikakulam. It is situated between N E and N E Latitudes and Longitude as shown in figure1.the total geographical study area is nearly 20sq.km. The total population is around The average rainfall is mm. GEOLOGY About percent of the area in the Mandal is underlain by soft rocks comprising sandstones of Gondwana systems and occupied about 4089 Km. in the central part of the Mandal. Ground water occurs in these formations under Volume: 03 Special Issue: 16 ICPECDM-2014 Dec-2014, 13
2 semi-confined and confined conditions [5]. In general these formations have resulted to moderate to low productive aquifers. The ground water department has constructed 5 tube wells and irrigation Development Corporation has constructed a number of log tube wells in the area. BOUNDARIES OF STUDY AREA: North side: ridge pint/ hills, South side : Kandivalasa River East side : Coastal belt and West side: stream shows the approximate resistivity ranges of some common rocks and water types in the basement complex area. Table 1: Approximate resistivity ranges for various rock and water types in the Basement Complex area [7] Rock type Resistivity (Ωm) Clay and marl 1 67 Topsoil Clayey soil Sandy Soil Limestone Sandstone Sand and gravels Schist Granite Surface water (in igneous rock) Groundwater (in igneous rock) Weathered laterite Fresh Laterite Weathered/fractured basement Fresh basement >1000 Fig.1 Study area of Pydibhimavaram THEORY AND PRINCIPLE OF ELECTRICAL RESISTIVITY SOUNDING Electrical resistivity techniques are based on the response of the earth to the flow of electric current. With an electrical current passed into the ground and two potential electrodes to record the resultant potential difference between them, we can obtain a direct measure of electrical impedance of the subsurface material. The resistivity of the subsurface material observed is a function of the magnitude of the current, the recorded potential difference and the geometry of the electrode array used. Measurement of resistivity is, in general, a measure of water saturation and pore space connectivity. Resistivity measurements are associated with varying depths relative to the distance between the current and potential electrodes in the survey, and can be interpreted qualitatively and quantitatively in terms of a litho logic and/or geohydrologic model of the subsurface [6].Electrical resistivity method involves the supply of direct current or low-frequency alternating current into the ground through a pair of current electrodes and the measurement of the resulting potential through another pair of electrode called potential electrodes. Rock resistivity depends on a number of factors such as the amount of water present in fractures and features, porosity and the degree of saturation. Table 1 RESULTS Volume: 03 Special Issue: 16 ICPECDM-2014 Dec-2014, 14 (i) GEO-ELECTRIC SECTIONS A visual inspection of all the geo-electric sections shows that three distinct litho logical units could be identified by the field mapping. A brief description of the two geoelectric sections obtained is as follows: Fig 2 Geo-electric Section normal to coast
3 Profile 1: Locations 4, 5, 6 are considered for generating a pseudo-section as they are collinear. At Station-5 (L-5 in Fig.4) the low resistivity zone is partly sandwiched in between layers of high resistivity. The anomaly begins at Station-4 and extends to Station-5 which indicates the possible existence of weathered material. By augmenting the geological reference of the study area the zone can be inferred as alluvial deposit. This low resistivity anomaly extends further into the Station-6 which has a gradual increment in the resistivity values as one ascends downwards. At greater depths the resistivity value is inexplicably high indicating rock strata. Fig.3 Geo-electric Section Parallel to River GEO-ELECTRIC SECTION PERPENDICULARS TO COASTAL BELT This consists of VESs 1,2&7 as shown in Figure 3. It is acquired Perpendiculars to coast direction (see Figure 1) and consists of three geo-electric layers. The first layer, the topsoil is characterized by layer with resistivity values from 13.7 to 34.9 Ohm.m and its thickness is between to 1.05m. The second layer underneath VESs 1 is suggestive of weathered granite and the remaining two VES 2&6 are Weathered or fractured Khondolite with resistivities ranging from 12.2 to 10.4 Ohm.m. The thicknesses vary from 6.44 to 8.16m. The third layer for all the VESs is Hard rock or electrical basement [8]. The resistivity ranging from 6.49 to 7.85 Ohm.m. The thicknesses vary from 6.44 to 17.7m GEO-ELECTRIC SECTION PARALLEL TO KANDIVALASA RIVER It comprises of three VES points (i.e. VES 4, 5&6) acquired approximately parallel to Kandivalasa river direction. The geo-electric section reveals three to three geo-electric layers (see Figure 4). The first layer, topsoil, is composed of Dry Sandy, Silt/Clayey having resistivity values ranging from 14.9 to 37.8 Ohm.m with thicknesses of 0.5 to 0.518m. The second layer beneath VESs 4, 5, and 6 is composed of Weathered or fractured Khondolitewith resistivity values ranging from 6.61 to 13.9 Ohm.m and layer thicknesses in the range of 1.38 to 13.3 m. The third layer for the VESs points 4&5having semi weathered gneiss and resistivity ranging from 12.5 to 17.9 Ohm.m. VESs points 6 having semi weathered gneiss overlying the hard rock, resistivity is 78.3 Ohm.m The thicknesses is infinity. (ii) PSEUDO-SECTIONS: Pseudo sections have been generated for the VES profiles. Points which are collinear or roughly collinear are considered for generating a Pseudo Section so as to portray the variation of resistivity across the points considered in a profile. Fig.4 Profile -1 Pseudo Section of 4, 5, 6 Fig.5. Profile -2 Pseudo Section of 7, 8, 5 Fig.6. Profile -5 Pseudo Section of 1, 2, 7 Volume: 03 Special Issue: 16 ICPECDM-2014 Dec-2014, 15
4 Fig.7 Profile 1, Resistivity Section of 1, 2, 7 Profile 2: Locations 7, 8, 5 are considered for this pseudo - section show in fig 5. Evidently, at Station-7 (from Fig.5) the trend in resistivity is increasing at the top layers and decreases as one ascends downwards. But again at higher depths the anomaly is increasing. The resistivity values suddenly increase from a marginal range of 10 to 15 ohmmeter to a range of 20 to 25 ohm-meters at a depth of 60 meters. This indicates a sudden change in the layers leading to denser strata. Much of the portion has the same loose deposit extending greater depths and hence the low resistivity anomaly is sandwiched between two layers of high resistivity. These loose sediment depositories could preferably be Alluvium and Lacustrine deposits which can be inferred from the geology of the study area. These are possible zones of aquifer existence. Profile 3 : Stations 1, 2, 7 are considered for the Pseudo Section as shown in fig.6. The Pseudo-Section for the points 1, 2 and 7 has a different trend than that of the others. Exactly under Station-1 (fig.6 ) the resistivity values are haphazard in variation. Prominently the low resistivity zones lie in the range of 1metre to 25metres.Wherin the case of Station points 2 and 7 the resistivity profiles can be juxtaposed in comparison. There s a mild visible difference and the low resistivity anomaly continues from Station point 1 to Station point 7 throughout in a similar fashion. Fig.8.Profile 2 Resistivity Section of 4, 5, 6 The southernmost region of the profile has highly resistive material which could be composed of hard rock formations. The highly weathered low resistivity zone is sandwiched in between the high resistive layers. (iii) RESISTIVITY SECTIONS Fig.9 Profile 2Resistivity Section of 7, 8, 5 Locations 4, 5, 6 are considered for generating a pseudosection as they are collinear. At Station-5 (L-5 in Fig.4) the low resistivity zone is partly sandwiched in between layers of high resistivity. The anomaly begins at Station-4 and extends to Station-5 which indicates the possible existence of weathered material. By augmenting the geological reference of the study area the zone can be inferred as alluvial deposit. This low resistivity anomaly extends further into the Station-6 which has a gradual increment in the resistivity values as one ascends downwards. At greater depths the resistivity value is inexplicably high indicating rock strata. Resistivity sections are generated for the same Stations for which pseudo sections have been generated. Profile 1: Stations 1, 2, 7 have been chosen for generating the section shown in fig.7. Clearly the resistivity trends initially increase, then decrease and again show a steep increase, which marks the occurrence of hard strata at the very deeper layers or partially weathered and poorly weathered strata.the layers having low resistivity imply less dense or loose strata in these regions. Profile 2: Stations 4, 5, 6 are considered for generating a Resistivity Section of the above profile shown in fig.8.below Station 4, the resistivity values are moderate with a sudden decrease at greater depths. The low resistivity anomaly is sandwiched between high resistivity layers. It extends horizontally throughout the profile. Profile 3: Stations 7, 8, 5 are considered for this section as shown in fig.9.at Station-8 (fig.9 ) the resistivity gradually increases and remains constant throughout the depth of the strata. This shows partially weathered rock which may or may not serve as a ground water prospective zone. Further, as one goes to Station-5 the low resistivity anomaly is persistent which repeats itself at Station-7. These may serve as ground water prospective zones as these low resistivity zones are a possible result of good weathering action. Volume: 03 Special Issue: 16 ICPECDM-2014 Dec-2014, 16
5 CONCLUSION In this study, electrical resistivity method using VES survey was carried out at thirteen locations in the study area using the Schlumberger electrode array with a view to understand the subsurface geologic settings that could guide the successful exploration of groundwater. Analysis of the interpreted results revealed the nature and composition of the subsurface lithologic units. Pseudo-sections and resistivity-sections were generated. Both low and high resistivity anomalies have been demarcated in pseudosection and resistivity sections. Majority of the VES curves are H type with multi layered geo-electrical sections. From the pseudo-sections it may be revealed that the NW and SW regions are comparatively more weathered than the other parts. Prominent low resistivity anomaly has been exhibited in all the pseudo-section profile (with an exception of Profile 5) indicating more weathered nature of the formation. Ibadan, Southwestern Nigeria.Journal of Science (2013) Vol. 1 No. 1: pp ACKNOWLEDGEMENTS The Authors are thankful to the Department of Science and Technology (DST), Ministry of Science& Technology, New Delhi, Government of India, for granting necessary financial assistances to carry out this research project work. REFERENCES [1] Pudentiana Okafor and Luke Mamah- Integration of Geophysical Techniques for Groundwater Potential Investigation in Katsina-Ala, Benue State, Nigeria. The Pacific Journal of Science and Technology,Volume 13. Number 2. November 2012 [2] L. A. Sunmonu.et.al- The groundwater potential evaluation at industrial estate Ogbomoso, Southwestern Nigeria. RMZ Materials and Geoenvironment, Vol. 59, No. 4, pp , 2012 [3] Mansour A. Al-Garni Geophysical Investigations for Groundwater in a Complex Subsurface Terrain,Wadi Fatima, KSA: A Case History Jordan Journal of Civil Engineering, Volume 3, No. 2, 2009 [4] B.S. Jatau- The Use of Vertical Electrical Sounding (VES) for Subsurface Geophysical Investigation around Bomo Area, Kaduna State, Nigeria.IOSR Journal of Engineering. Vol. 3, Issue 1 (Jan. 2013), PP [5] Ogundana, A.K and Talabi A. O- Ground water Potential Evaluation of Ultra Modern Guest House, Afe Babalola University, Ado-Ekiti, Southwestern Nigeria. The International Journal Of Engineering And Science (IJES) Volume 3 Pages 41-5,2014 [6] A. N. Amadi- Evaluation of the Groundwater Potential inpompo Village, Gidan Kwano, Minna Using Vertical Electrical Resistivity Sounding. British Journal of Applied Science & Technology 1(3): 53-66, 2011 [7] Telford, W.N., Geldart, L.P., Shriff, R.E. (2001). Applied Geophysics (2nd Ed.). Cambridge University press, Cambridge,770pp. [8] Kehinde Ishola1 et.al- Assessing Groundwater Potential Zones in Basement Complex Terrain Using Resistivity Depth Soundings: A Case of Challenge and Oluyole in Volume: 03 Special Issue: 16 ICPECDM-2014 Dec-2014, 17
The Use of Vertical Electrical Sounding (VES) for Subsurface Geophysical Investigation around Bomo Area, Kaduna State, Nigeria
IOSR Journal of Engineering (IOSRJEN) e-issn: 2250-3021, p-issn: 2278-8719 Vol. 3, Issue 1 (Jan. 2013), V4 PP 10-15 The Use of Vertical Electrical Sounding (VES) for Subsurface Geophysical Investigation
More informationVertical electrical sounding (VES) for subsurface geophysical investigation in Kanigiri area, Prakasam district, Andhra Pradesh, India
Available online at www.pelagiaresearchlibrary.com Advances in Applied Science Research, 2014, 5(5):82-86 ISSN: 0976-8610 CODEN (USA): AASRFC Vertical electrical sounding (VES) for subsurface geophysical
More information2-D RESISTIVITY IMAGING SURVEY FOR WATER-SUPPLY TUBE WELLS IN A BASEMENT COMPLEX: A CASE STUDY OF OOU CAMPUS, AGO-IWOYE SW NIGERIA
2-D RESISTIVITY IMAGING SURVEY FOR WATER-SUPPLY TUBE WELLS IN A BASEMENT COMPLEX: A CASE STUDY OF OOU CAMPUS, AGO-IWOYE SW NIGERIA 1 AYOLABI, Elijah Adebowale. 2 FOLORUNSO, Adetayo Femi. and 3 ARIYO, Stephen
More informationGroundwater Exploration In Parts Of Mangu- Halle North-Central Nigeria.
International Journal of Scientific and Research Publications, Volume 7, Issue 10, October 2017 440 Groundwater Exploration In Parts Of Mangu- Halle North-Central Nigeria. I. Mamuda *, P.M. Akushai **
More informationGround Magnetic and Electrical Resistivity Mapping for Basement Structurs over Charnokitic Terrain in Ado-Ekiti Area, Southwestern Nigeria
International Journal of Science and Technology Volume 3 No. 10, October, 2014 Ground Magnetic and Electrical Resistivity Mapping for Basement Structurs over Charnokitic Terrain in Ado-Ekiti Area, Southwestern
More informationMICRO LEVEL GEO-RESISTIVITY SURVEY THROUGH V.E.S. TEST FOR GROUNDWATER FEASIBILITY STUDY AND SELECTION OF BORE WELL SITES IN PIPILI BLOCK OF PURI
Review of Environment and Earth Sciences 2014 Vol.1, No.2, pp. 37-45 ISSN(e): 2313-8440 ISSN(p): 2409-2150 DOI: 10.18488/journal.80/2014.1.2/80.2.37.45 MICRO LEVEL GEO-RESISTIVITY SURVEY THROUGH V.E.S.
More informationHydro-Geophysical Study of River Niger Floodplain at Jebba-North, Nigeria
Journal of Emerging Trends in Engineering and Applied Sciences (JETEAS) 3 (1): 152-158 Scholarlink Research Institute Journals, 212 (ISSN: 2141-716) jeteas.scholarlinkresearch.org Journal of Emerging Trends
More informationMorenikeji P. Anjorin, B.Tech. 1 and Martins O. Olorunfemi, Ph.D. 2*
A Short Note on Comparative Study of Schlumberger and Half Schlumberger Arrays in Vertical Electrical Sounding in a Basement Complex Terrain of Southwest Nigeria. Morenikeji P. Anjorin, B.Tech. 1 and Martins
More informationFIG. 1 TOPOLOGY MAP SHOWING THE SURVEY AREA.
SCIENCE WORLD JOURNAL VOL 2 (NO3) 2007 FULL LENGTH RESEARCH ARTICLE A REGIONAL GEOELECTRIC INVESTIGATION FOR GROUNDWATER EXPLORATION IN MINNA AREA, NORTH WEST NIGERIA. MOHAMMED, L. N. 1, *ABOH, H. O. 2
More informationScholars Research Library
Available online at www.scholarsresearchlibrary.com Scholars Research Library Archives of Physics Research, 2010, 1 (2):37-45 (http://scholarsresearchlibrary.com/archive.html) ISSN 0976-0970 2-D Resistivity
More informationGroundwater Assessment in Apapa Coast-Line Area of Lagos Using Electrical Resistivity Method
Journal of Emerging Trends in Engineering and Applied Sciences (JETEAS) 2 (4): 673-679 Scholarlink Research Institute Journals, 2011 (ISSN: 2141-7016) jeteas.scholarlinkresearch.org Groundwater Assessment
More informationRESISTIVITY IMAGING AND BOREHOLE INVESTIGATION OF THE BANTING AREA AQUIFER, SELANGOR, MALAYSIA. A.N. Ibrahim Z.Z.T. Harith M.N.M.
JOURNAL OF ENVIRONMENTAL HYDROLOGY The Electronic Journal of the International Association for Environmental Hydrology On the World Wide Web at http://www.hydroweb.com VOLUME 11 2003 RESISTIVITY IMAGING
More informationGeophysical Investigation of a Suspected Foundation Failure at Ogbomoso, Southwestern, Nigeria.
Geophysical Investigation of a Suspected Foundation Failure at Ogbomoso, Southwestern, Nigeria. Enoch E. Sangodiji, M.Sc. and Martins O. Olorunfemi, Ph.D. Department of Applied Geophysics, Federal University
More informationEVALUATION OF GROUNDWATER POTENTIAL USING ELECTRICAL RESISTIVITY METHOD IN OKENUGBO AREA, AGO - IWOYE, SOUTHWESTERN, NIGERIA.
EVALUATION OF GROUNDWATER POTENTIAL USING ELECTRICAL RESISTIVITY METHOD IN OKENUGBO AREA, AGO - IWOYE, SOUTHWESTERN, NIGERIA. OLADUNJOYE H.T., 1 ODUNAIKE R.K., 1 OGUNSOLA P 1. OLALEYE O.A. 2 1 DEPARTMENT
More informationRelevance of 2D Electrical Imaging in Subsurface Mapping: Case Study of National Animal Production Research Institute (NAPRI), Zaria.
Relevance of 2D Electrical Imaging in Subsurface Mapping: Case Study of National Animal Production Research Institute (NAPRI), Zaria. S.I. Fadele, Ph.D. (in view) 1* ; J. Adamu, M.Sc. 2 ; N.O. Patrick,
More informationS.I. Fadele, M.Sc. 1 ; P.O. Sule, Ph.D. 1 ; and B.B.M. Dewu, Ph.D * ABSTRACT
The Use of Vertical Electrical Sounding (VES) for Groundwater Exploration around Nigerian College of Aviation Technology (NCAT), Zaria, Kaduna State, Nigeria. S.I. Fadele, M.Sc. 1 ; P.O. Sule, Ph.D. 1
More informationAPPLICATION OF ELECTRICAL RESISTIVITY TOMOGRAPHY FOR SAND UNDERWATER EXTRACTION
International Scientific Conference GEOBALCANICA 2018 APPLICATION OF ELECTRICAL RESISTIVITY TOMOGRAPHY FOR SAND UNDERWATER EXTRACTION Maya Grigorova Ivaylo Koprev University of Mining and Geology St. Ivan
More informationGROUNDWATER CONFIGURATION IN THE UPPER CATCHMENT OF MEGHADRIGEDDA RESERVOIR, VISAKHAPATNAM DISTRICT, ANDHRA PRADESH
GROUNDWATER CONFIGURATION IN THE UPPER CATCHMENT OF MEGHADRIGEDDA RESERVOIR, VISAKHAPATNAM DISTRICT, ANDHRA PRADESH Prof.P.Jagadeesara Rao Department of Geo-Engineering and Centre for Remote Sensing, College
More informationIndex Terms- Apparent Resistivity, Aquifer, Geoelectric Section, Piezometric Surface.
Investigation of Groundwater Resources of Rafin Guza Area of Kaduna, Nigeria using Resistivity Method Olaniyan, Isaac O, Olorunnaiye, Emmanuel S. Abstract - The groundwater resources of Rafin Guza village
More informationSubsurface Characterization using Electrical Resistivity(Dipole-Dipole) method at Lagos State University (LASU) Foundation School, Badagry
Available online at www.pelagiaresearchlibrary.com Advances in Applied Science Research, 2010, 1 (1): 174-181 Subsurface Characterization using Electrical Resistivity(Dipole-Dipole) method at Lagos State
More informationElijah Adebowale Ayolabi, Ph.D. 1, Adetayo Femi Folorunso, M.Sc. 2*, Ayodele Franklin Eleyinmi, B.Sc. 1, and Esther O. Anuyah, B.Sc.
Applications of 1D and 2D Electrical Resistivity Methods to Map Aquifers in a Complex Geologic Terrain of Foursquare Camp, Ajebo, Southwestern Nigeria. Elijah Adebowale Ayolabi, Ph.D. 1, Adetayo Femi Folorunso,
More informationVertical Electrical Sounding Survey for Groundwater Exploration in Parts of Anyigba and its Environs, in the Anambra Basin of Nigeria
British Journal of Applied Science & Technology 4(): 978-988, 204 SCIENCEDOMAIN international www.sciencedomain.org Vertical Electrical Sounding Survey for Groundwater Exploration in Parts of and its Environs,
More informationEthiopian Journal of Environmental Studies and Management Vol. 6 No
APPLICATION OF ELECTRICAL RESISTIVITY SURVEY FOR GROUNDWATER INVESTIGATION IN A BASEMENT ROCK REGION: A CASE STUDY OF AKOBO - IBADAN, NIGERIA * NWANKWO, L.I., 1 OLASEHINDE, P.I. 2 and OSUNDELE, O.E. 1
More informationAnalysis of electrical resistivity data for the determination of aquifer depth at Sapele RD in Benin city
Available online at www.pelagiaresearchlibrary.com Advances in Applied Science Research, 203, 4(6):268-276 ISSN: 0976-860 CODEN (USA): AASRFC Analysis of electrical resistivity data for the determination
More informationINTEGRATED GEOPHYSICAL INVESTIGATION OF SEQUENCE OF DEPOSITION OF SEDIMENTARY STRATA IN ABAKALIKI, NIGERIA ABSTRACT
INTEGRATED GEOPHYSICAL INVESTIGATION OF SEQUENCE OF DEPOSITION OF SEDIMENTARY STRATA IN ABAKALIKI, NIGERIA Agha S.O Dept. of Industrial Physics Ebonyi State University, Abakaliki, Nigeria & Arua A.I Dept.
More informationIdentification of aquifer zones by VES method: A case study from Mangalore block, Tamil Nadu, S. India
Available online at www.scholarsresearchlibrary.com Scholars Research Library Archives of Applied Science Research, 011, 3 ():414-41 (http://scholarsresearchlibrary.com/archive.html) ISSN 0975-508X CODEN
More informationFINAL REPORT GEOPHYSICAL INVESTIGATION VILLAGE ALHAMBRA RETENTION POND SITE THE VILLAGES, FLORIDA
FINAL REPORT GEOPHYSICAL INVESTIGATION VILLAGE ALHAMBRA RETENTION POND SITE THE VILLAGES, FLORIDA Prepared for Andreyev Engineering, Inc. Oxford, FL Prepared by GeoView, Inc. St. Petersburg, FL August
More informationHydro-Geophysical Investigation of the Federal Housing Estate Akure, Southwestern Nigeria
Journal of Emerging Trends in Engineering and Applied Sciences (JETEAS) 4(6): 793-799 Scholarlink Research Institute Journals, 2013 (ISSN: 2141-7016) jeteas.scholarlinkresearch.org Journal of Emerging
More informationAN INTEGRATED GEOPHYSICAL INVESTIGATION OF A SPRING IN IBUJI, IGBARA-OKE, SOUTHWESTERN NIGERIA.
Ife Journal of Science vol. 13, no. 1 (2011) AN INTEGRATED GEOPHYSICAL INVESTIGATION OF A SPRING IN IBUJI, IGBARA-OKE, SOUTHWESTERN NIGERIA. 63 Bayode S. * and Akpoarebe O. Department of Applied Geophysics,
More informationAssessment of Ground Water in a Part of Coastal West Bengal using Geo-Electrical Method
Vol. 13, No. 2, pp. 203-210 (2013) Journal of Agricultural Physics ISSN 0973-032X http://www.agrophysics.in Research Article Assessment of Ground Water in a Part of Coastal West Bengal using Geo-Electrical
More informationGeophysical Investigation of Foundation Condition of A Site in Ikere- Ekiti, Ekiti State, South-Western Nigeria
Australian Journal of Basic and Applied Sciences, 5(9): 1852-1857, 2011 ISSN 1991-8178 Geophysical Investigation of Foundation Condition of A Site in Ikere- Ekiti, Ekiti State, South-Western Nigeria 1
More informationDetermination of Thickness of Aquifer with Vertical Electrical Sounding
IOSR Journal of Mechanical and Civil Engineering (IOSR-JMCE) e-issn: 2278-1684,p-ISSN: 2320-334X, Volume 12, Issue 6 Ver. IV (Nov. - Dec. 2015), PP 52-56 www.iosrjournals.org Determination of Thickness
More informationGeophysical Investigation: A Case Study of Basement Complex, Nigeria
Geophysical Investigation: A Case Study of Basement Complex, Nigeria Adiela U.P 1, Ayodele Moses Oyewole 2 and Omoirabor Omoleomo 3 1 Department of Petroleum Engineering, Nigerian Agip Oil Company, Port
More informationCauses of Borehole Failure in Complex Basement Terrains: ABUAD Case Study, Southwestern Nigeria. w w w. a j e r. o r g Page 192
American Journal of Engineering Research (AJER) e-issn: 2320-0847 p-issn : 2320-0936 Volume-4, Issue-10, pp-192-201 www.ajer.org Research Paper Open Access Causes of Borehole Failure in Complex Basement
More informationInternational Journal of Basic and Applied Sciences Raibu et. al., Vol. 1 No. 2 ISSN: (A peer reviewed International Journal)
(A peer reviewed International Journal) Determination of Aquifer Layer by the Application of Electrical Resistivity and Electromagnetic Method of Exploration at Ojoo Town Oyo State Southwestern Nigeria
More informationAdebayo O. Ojo, M.Sc. 1* and Martins O. Olorunfemi, Ph.D *
A Graphical and Semi-Quantitative Technique for Investigating Vertical Electrical Sounding (VES) Curves for Indices of Confined Fractured Basement Column. Adebayo O. Ojo, M.Sc. 1* and Martins O. Olorunfemi,
More informationCHARACTERIZATION OF SOIL PROFILE OF DHAKA CITY USING ELECTRICAL RESISTIVITY TOMOGRAPHY (ERT)
CHARACTERIZATION OF SOIL PROFILE OF DHAKA CITY USING ELECTRICAL RESISTIVITY TOMOGRAPHY (ERT) Mehedi Ahmed ANSARY 1, B.S. Pushpendue BISWAS 2 and Abul KHAIR 3 1 Professor, Department of Civil Engineering
More informationDELINEATION OF FRESH-BRACKISH WATER AND BRACKISH-SALINE WATER INTERFACES USING VES SOUNDINGS IN SHANI, BORNO STATE, NIGERIA
JOURNAL OF ENVIRONMENTAL HYDROLOGY The Electronic Journal of the International Association for Environmental Hydrology On the World Wide Web at http://www.hydroweb.com VOLUME 19 2011 DELINEATION OF FRESH-BRACKISH
More informationGEOTECHNICAL INVESTIGATION OF THE SUBSURFACE FORMATIONS, USING ELECTRICAL RESISTIVITY METHOD IN NORTHERN PART OF PAIKO TOWN, NIGER STATE, NIGERIA
GEOTECHNICAL INTIGATION OF THE SUBSURFACE FORMATIONS, USING ELECTRICAL RESISTIVITY METHOD IN NORTHERN PART OF PAIKO TOWN, NIGER STATE, NIGERIA Supported by D. U. Alhassan 1 *, D. N. Obiora 2 and F. N.
More informationApplication of Remote Sensing and Geo-Electrical Method for Groundwater Exploration in Khor Al Alabyad, North Kordofan State, Sudan
American Journal of Earth Sciences 2015; 2(6): 242-246 Published online January 10, 2016 (http://www.openscienceonline.com/journal/ajes) ISSN: 2381-4624 (Print); ISSN: 2381-4632 (Online) Application of
More informationGEO-ELECTRIC INVESTIGATION OF THE GROUNDWATER POTENTIAL DISTRIBUTION WITHIN GWALE LOCAL GOVERNMENT AREA OF KANO STATE NIGERIA
GEO-ELECTRIC INVESTIGATION OF THE GROUNDWATER POTENTIAL DISTRIBUTION WITHIN GWALE LOCAL GOVERNMENT AREA OF KANO STATE NIGERIA Full Length Research Article A.M. Idris, 2* G. Ahmed, 3 A. L. Ahmed, 3 K. M.
More informationK. A. Murana, P. Sule, A.L. Ahmed, E.M. Abraham and E.G. Obande. 1. Introduction
Subsurface stratigraphic mapping using geoelectric method and its impact on development in Federal College of Education (technical) Gusau, Zamfara State, Nigeria K. A. Murana, P. Sule, A.L. Ahmed, E.M.
More informationCHAPTER 9 SUMMARY AND CONCLUSIONS
CHAPTER 9 SUMMARY AND CONCLUSIONS The following are the important conclusions and salient features of the present study. 1. The evaluation of groundwater potential is a prerequisite for any kind of planning
More informationSEISMIC REFRACTION INVESTIGATION OF THE SUBSURFACE STRUCTURE AT THE SOUTHERN PART OF NIGER STATE COLLEGE OF EDUCATION, MINNA, NIGERIA
Bayero Journal of Pure and Applied Sciences, 3(2): 56-6 Received: May, 200 Accepted: October, 200 ISSN 2006-6996 SEISMIC REFRACTION INVESTIGATION OF TE SUBSURFACE STRUCTURE AT TE SOUTERN PART OF NIGER
More informationTWO DIMENSIONAL ELECTRICAL IMAGING OF THE SUBSURFACE STRUCTURE OF BOMO DAM ZARIA, KADUNA STATE NORTH CENTRAL NIGERIA
TWO DIMENSIONAL ELECTRICAL IMAGING OF THE SUBSURFACE STRUCTURE OF BOMO DAM ZARIA, KADUNA STATE NORTH CENTRAL NIGERIA Felix O. Ojo, Department of Geology, Ekiti State University, Ado-Ekiti, Nigeria. Oladimeji
More informationINTERNATIONAL JOURNAL OF SCIENTIFIC & TECHNOLOGY RESEARCH VOLUME 3, ISSUE 10, OCTOBER 2014 ISSN
Integrated Geophysical Investigations For The Development Of A Sustainable Water Supply Scheme Within The Ekiti State University Campus, Ado-Ekiti, Southwestern Nigeria Eluwole A. Bolaji, Ademilua O. Lawrence
More informationGroundwater Potential Evaluation of College of Engineering, Afe Babalola University, Ado-Ekiti, Southwestern Nigeria
American Journal of Water Resources, 2014, Vol. 2, No. 1, 2530 Available online at http://pubs.sciepub.com/ajwr/2/1/4 Science and Education Publishing DOI:10.12691/ajwr214 Groundwater Potential Evaluation
More information3D Electrical Resistivity Tomography (ERT) Survey of a Typical Basement Complex Terrain
Journal of Emerging Trends in Engineering and Applied Sciences (JETEAS) 2 (4): 680-686 Scholarlink Research Institute Journals, 2011 (ISSN: 2141-7016) jeteas.scholarlinkresearch.org Journal of Emerging
More informationINTERNATIONAL JOURNAL OF GEOMATICS AND GEOSCIENCES Volume 3, No 1, 2012
INTERNATIONAL JOURNAL OF GEOMATICS AND GEOSCIENCES Volume 3, No 1, 2012 Copyright by the authors - Licensee IPA- Under Creative Commons license 3.0 Research article ISSN 0976 4380 Groundwater potential
More informationGroundwater Sustainability at Wadi Al Bih Dam, Ras El Khaimah, United Arab Emirates (UAE) using Geophysical methods
Groundwater Sustainability at Wadi Al Bih Dam, Ras El Khaimah, United Arab Emirates (UAE) using Geophysical methods Ahmed Murad, Amir Gabr, Saber Mahmoud, Hasan Arman & Abdulla Al Dhuhoori Geology Department
More informationDelineation of Groundwater Prospective Zones by Schlumberger electrode array in Bangriposi block of Odisha
International Research Journal of Earth Sciences ISSN 2321 2527 Int. Res.J. Earth Sci. Delineation of Groundwater Prospective Zones by Schlumberger electrode array in Bangriposi block of Odisha Abstract
More informationAN APPRAISAL OF CERTAIN CHARACTERISTICS OF AQUIFER IN CHIKUN LOCAL GOVERNMENT AREA OF KADUNA, NIGERIA
AN APPRAISAL OF CERTAIN CHARACTERISTICS OF AQUIFER IN CHIKUN LOCAL GOVERNMENT AREA OF KADUNA, NIGERIA Isaac Oladejo Olaniyan 1 and Johnson Nimmo Tsuzom 2 1 Department of Physical Sciences, Ondo State University
More informationGeophysical Study of Limestone Attributes At Abudu Area of Edo State, Nigeria
Journal of Emerging Trends in Engineering and Applied Sciences (JETEAS) 2 (5): 795-800 Scholarlink Research Institute Journals, 2011 (ISSN: 2141-7016) jeteas.scholarlinkresearch.org Journal of Emerging
More informationAzimuthal Square Array Configuration and Groundwater Prospecting in Quartzite Terrian at Edaikkal, Ambasamudram, Tirunelveli
Research Journal of Earth Sciences 4 (2): 49-55, 2012 ISSN 1995-9044 IDOSI Publications, 2012 DOI: 10.5829/idosi.rjes.2012.4.2.2937 Azimuthal Square Array Configuration and Groundwater Prospecting in Quartzite
More informationInvestigation of Underground Water at Paiko Using Vertical Electrical Sounding Technique in Paiko, Nigeria
Investigation of Underground Water at Paiko Using Vertical Electrical Sounding Technique in Paiko, Nigeria Mamman H. Mamman and Ojo T. John Department of Science Technology, Federal Polytechnic, Ado-Ekiti,
More informationGeophysical Investigation of Ground Water Using Vertical Electrical Sounding and Seismic Refraction Methods
International Journal of Petroleum and Petrochemical Engineering (IJPPE) Volume 2, Issue 1, 2016, PP 6-11 ISSN 2454-7980 (Online) www.arcjournals.org Geophysical Investigation of Ground Water Using Vertical
More information1-D Electrical Resistivity Survey For Groundwater In Ketu-Adie Owe, Ogun State, Nigeria.
IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG) e-issn: 2321 0990, p-issn: 2321 0982.Volume 3, Issue 5 Ver. I (Sep. - Oct. 2015), PP 75-82 www.iosrjournals.org 1-D Electrical Resistivity Survey
More informationIntegration of Seismic Refraction and 2D Electrical Resistivity in Locating Geological Contact
Open Journal of Geology, 2013, 3, 7-12 doi:10.4236/ojg.2013.32b002 Published Online April 2013 (http://www.scirp.org/journal/ojg) Integration of Seismic Refraction and 2D Electrical Resistivity in Locating
More informationRelevance of Geophysics in Road Failures Investigation in a Typical Basement Complex of Southwestern Nigeria.
Relevance of Geophysics in Road Failures Investigation in a Typical Basement Complex of Southwestern Nigeria. K.A.N. Adiat, M.Tech. *, A.O. Adelusi, Ph.D., and M.A. Ayuk, M.Tech. Department of Applied
More informationD.C. RESISTIVITY INVESTIGATION OF SUBSURFACE LAYERING FOR GEOTECHNICAL APPLICATION IN MILLENNIUM CITY, KADUNA, KADUNA STATE.
Full Length Research Article D.C. RESISTIVITY IVESTIGATIO OF SUBSURFACE LAYERIG FOR GEOTECHICAL APPLICATIO I MILLEIUM CITY, KADUA, KADUA STATE. Dogara M. D., Aboh H. O. and Kogi K. A. Department of Physics,
More informationRESISTIVITY IMAGING IN EASTERN NEVADA USING THE AUDIOMAGNETOTELLURIC METHOD FOR HYDROGEOLOGIC FRAMEWORK STUDIES. Abstract.
RESISTIVITY IMAGING IN EASTERN NEVADA USING THE AUDIOMAGNETOTELLURIC METHOD FOR HYDROGEOLOGIC FRAMEWORK STUDIES Darcy K. McPhee, U.S. Geological Survey, Menlo Park, CA Louise Pellerin, Green Engineering,
More informationEvaluation of Subsurface Formation of Pabna District, Bangladesh
IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG) e-issn: 2321 0990, p-issn: 2321 0982.Volume 1, Issue 4 (Sep. Oct. 2013), PP 30-36 Evaluation of Subsurface Formation of Pabna District, Bangladesh
More informationENGINEERING GEOPHYSICAL STUDY OF THE CONVOCATION SQUARE, KADUNA STATE UNIVERSITY.
ENGINEERING GEOPHYSICAL STUDY OF THE CONVOCATION SQUARE, KADUNA STATE UNIVERSITY. N.K.Abdullahi 1, S.F.Ugbade 1, M.A.Abdullahi 2. Full Length Research Article 1 Department of Physics, Kaduna State University,
More informationInternational Journal of Scientific & Engineering Research, Volume 7, Issue 3, March ISSN
International Journal of Scientific & Engineering Research, Volume 7, Issue 3, March-2016 152 Investigation of Groundwater Resources by Determining the Aquifer Parameters around Futa Staff Quarters C.T.
More informationGEOELECTRICAL INVESTIGATION OF GROUNDWATER CONDITION IN OLEH, NIGERIA
www.arpapress.com/volumes/vol15issue1/ijrras_15_1_14.pdf GEOELECTRICAL INVESTIGATION OF GROUNDWATER CONDITION IN OLEH, NIGERIA O. Anomohanran Physics Department, Delta State University, Abraka, Delta State,
More informationScholars Research Library. Geophysical investigation of effects of topographic complexities on groundwater potential in Ibusa, Delta State Nigeria
Available online at www.scholarsresearchlibrary.com Scholars Research Library Archives of Physics Research, 010, 1 (3):6-71 (http://scholarsresearchlibrary.com/archive.html) ISSN 0976-0970 CODEN (USA):
More informationGeophysical Investigation of the Precambrian Marble Occurrence in Itobe Area, Central Nigeria
British Journal of Applied Science & Technology 4(13): 1891-1904, 2014 SCIENCEDOMAIN international www.sciencedomain.org Geophysical Investigation of the Precambrian Marble Occurrence in Itobe Area, Central
More informationGeological and Geophysical Investigation of Groundwater in Parts of Paiko, Sheet 185, North-Central Nigeria
International Journal of Engineering Research and Development e-issn: 2278-067X, p-issn: 2278-800X, www.ijerd.com Volume 6, Issue 1 (February 2013), PP. 01-08 Geological and Geophysical Investigation of
More informationScholars Research Library
Available online at www.scholarsresearchlibrary.com Scholars Research Library Archives of Applied Science Research, 010, (): 4-34 (http://scholarsresearchlibrary.com/archive.html) ISSN 0975-508X CODEN
More informationGeophysical Investigation of Egbeta, Edo State, Nigeria, Using Electrical Resistivity Survey to Assess the Ground water Potential
368 Geophysical Investigation of Egbeta, Edo State, Nigeria, Using Electrical Resistivity Survey to Assess the Ground water Potential 1 Aigbogun, Christopher O., 1 Adegbite, Joseph, T., 2 Olorunsola,Kuforijimi,
More informationElectrical prospecting involves detection of surface effects produced by electrical current flow in the ground.
Electrical Surveys in Geophysics Electrical prospecting involves detection of surface effects produced by electrical current flow in the ground. Electrical resistivity method Induced polarization (IP)
More informationCharacterization of the geology and subsurface crystalline limestone mining using 2D ERI at Puthur Mines, Tirunelveli, Tamilnadu
Available online at www.scholarsresearchlibrary.com Archives of Applied Science Research, 2012, 4 (3):1261-1265 (http://scholarsresearchlibrary.com/archive.html) ISSN 0975-508X CODEN (USA) AASRC9 Characterization
More informationA Preliminary Geophysical Reconnaissance Mapping of Emirau Ground Water Resource, Emirau Island, New Ireland Province, PNG
A Preliminary Geophysical Reconnaissance Mapping of Emirau Ground Water Resource, Emirau Island, New Ireland Province, PNG Geological Survey Division of Mineral Resources Authority (MRA) Papua New Guinea
More informationPalaeoscars and landslide prediction using 2D ERI techniques in Ooty area, Nilgiri district, Tamilnadu
Available online at www.scholarsresearchlibrary.com Archives of Applied Science Research, 2012, 4 (1):262-268 (http://scholarsresearchlibrary.com/archive.html) ISSN 0975-508X CODEN (USA) AASRC9 Palaeoscars
More informationLECTURE 10. Module 3 : Field Tests in Rock 3.6 GEOPHYSICAL INVESTIGATION
LECTURE 10 3.6 GEOPHYSICAL INVESTIGATION In geophysical methods of site investigation, the application of the principles of physics are used to the study of the ground. The soil/rock have different characteristics
More informationASSESSMENT OF GROUNDWATER POTENTIAL IN ARUJO- RODI KOPANY AREA, HOMA BAY COUNTY, KENYA. NAME: AYETE DAVID OMAJILONG
ASSESSMENT OF GROUNDWATER POTENTIAL IN ARUJO- RODI KOPANY AREA, HOMA BAY COUNTY, KENYA. NAME: AYETE DAVID OMAJILONG SUMMARY. Groundwater development for portable water supply in Kenya for rural people
More informationGeoelectrical Investigation of Groundwater Potentials of Northern Paiko, Niger State, North Central Nigeria
Journal of Earth Science, Vol. 28, No. 1, p. 103 112, February 2017 ISSN 1674-487X Printed in China DOI: 10.1007/s12583-017-0748-2 Geoelectrical Investigation of Groundwater Potentials of Northern Paiko,
More informationInterpretation of Subsurface Geological Structure of Massepe Geothermal Area Using Resistivity Data
Proceedings World Geothermal Congress 2010 Bali, Indonesia, 25-29 April 2010 Interpretation of Subsurface Geological Structure of Massepe Geothermal Area Using Resistivity Data Ahmad Zarkasyi and Yuanno
More informationUse of VLF Electromagnetic and Electrical Resistivity Methods for Groundwater Investigation in Oke Amu Area, Southwestern Nigeria
International Journal of Research Studies in Science, Engineering and Technology Volume 3, Issue 10, October 2016, PP 1-10 ISSN 2349-4751 (Print) & ISSN 2349-476X (Online) Use of VLF Electromagnetic and
More informationPreliminary Geophysical Investigation of Orin Clay Deposit, Southwestern Nigeria: Deductions, Implications and Possible Applications
Preliminary Geophysical Investigation of Orin Clay Deposit, Southwestern Nigeria: Deductions, Implications and Possible Applications Oluwakunle Moyofoluwa Ogunsakin Department of Geology, Wesley University,
More informationGeophysical investigations for groundwater exploration in a crystalline basement, southwest Nigeria
Geophysical investigations for groundwater exploration in a crystalline basement, southwest Nigeria Awomeso Awonusi 1, Orebiyi Olabisi 1 and Oyedokun Olabamiji 2. 1 Department of Water Resources Management
More information1. Resistivity of rocks
RESISTIVITY 1) Resistivity of rocks 2) General principles of resistivity surveying 3) Field procedures, interpretation and examples 4) Summary and conclusions INDUCED POLARIZATION 1) General principles
More informationThe three-year mapping and monitoring of underground cavity expansion with 2D resistivity survey: What has revealed?
The three-year mapping and monitoring of underground cavity expansion with 2D resistivity survey: What has revealed? Peangta Satarugsa 1, Winit Youngmee 1 and Suvijuk Meesawat 1 1. Department of Geotechnology,
More informationWENNER ARRAY RESISTIVITY AND SP LOGGING FOR GROUND WATER EXPLORATION IN SAWERPURAM TERI DEPOSITS, THOOTHUKUDI DISTRICT, TAMIL NADU, INDIA
WENNER ARRAY RESISTIVITY AND SP LOGGING FOR GROUND WATER EXPLORATION IN SAWERPURAM TERI DEPOSITS, THOOTHUKUDI DISTRICT, TAMIL NADU, INDIA A. Antony Ravindran 1, N. Ramanujam 2 and P. Somasundaram 1 1 Department
More information[Penumaka, 7(1): January-March 2017] ISSN Impact Factor
INTERNATIONAL JOURNAL OF ENGINEERING SCIENCES &MANAGEMENT HYDROGEOMORPHOLOGY OF CHEVELLA BASIN, RANGA REDDY DISTRICT, TELANGANA STATE Penumaka Ramesh* 1 & Podila Sankara Pitchaiah 2 * 1&2 Department of
More informationUnderground water exploration of Oleh, Nigeria using the electrical resistivity method
Scientific Research and Essays Vol. 6(20), pp. 4295-4300, 19 September, 2011 Available online at http://www.academicjournals.org/sre ISSN 1992-2248 2011 Academic Journals Full Length Research Paper Underground
More information2-D Resistivity Study: The Horizontal Resolution Improvement by Introducing the Enhancing Horizontal Resolution (EHR) Technique
Open Journal of Geology, 213, 3, 1-6 doi:1.4236/ojg.213.32b1 Published Online April 213 (http://www.scirp.org/journal/ojg) 2-D Resistivity Study: The Horizontal Resolution Improvement by Introducing the
More informationELECTRICAL RESISTIVITY TOMOGRAPHY
NOTIO Association Clay Technological Centre C/ Río Cabriel s/n 45007 Toledo Tel.: 925 24 11 62 info@notio.es www.notio.es Page 1 / 7 SUMMARY 1. PHYSICAL FUNDAMENTALS OF THE... 3 1.1. ELECTRICAL BEHAVIOR
More informationVOL. 7, NO. 5, MAY 2012 ISSN ARPN Journal of Engineering and Applied Sciences
ELECTRICAL ANISOTROPY OF CRYSTALLINE BASEMENT/SEDIMENT ROCK AROUND IFON, SOUTH-WESTERN NIGERIA: IMPLICATIONS IN GEOLOGIC MAPPING AND GROUNDWATER INVESTIGATION F. A. Isife and R. A. Obasi Department of
More informationIntegration of Thematic Maps Through GIS for Identification of Groundwater Potential zones. Amaresh Kr. Singh & S. Ravi Prakash
Integration of Thematic Maps Through GIS for Identification of Groundwater Potential zones Amaresh Kr. Singh & S. Ravi Prakash Remote Sensing Applications Centre, U.P., Sector -G, Jankipuram, Lucknow rsacup@sancharnet.in,
More informationEVALUATION OF GROUNDWATER POTENTIAL OF ODEDA LOCAL GOVERNMENT AREA, OGUN STATE, SOUTHWEST NIGERIA
ISSN: Print 2277 0593 Online 2315 7461 FUNAAB 2016 EVALUATION OF GROUNDWATER POTENTIAL OF ODEDA LOCAL GOVERNMENT AREA, OGUN STATE, SOUTHWEST NIGERIA 1*V. MAKINDE, 2 A.O. ERUOLA, 1 S.A. GANIYU, 1 O.T. OLURIN,
More informationSUITABILITY OF ELECTRICAL RESISTIVITY SURVEY FOR SELECTING ANICUT SITE IN ORDER TO AUGMENT GROUND WATER A CASE STUDY
Annals of Arid Zone 30 (3) : 187-195, 1991 SUTABLTY OF ELECTRCAL RESSTVTY SURVEY FOR SELECTNG ANCUT STE N ORDER TO AUGMENT GROUND WATER A CASE STUDY J.P. SHUKLA* and S.M. PANDEY Ground Water Department,
More informationThe impact of geologic setting on the groundwater occurrence in the Eocene limestone of El Minia-East Nile-Egypt, using geoelectrical technique
Available online at www.pelagiaresearchlibrary.com Advances in Applied Science Research, 2016, 7(4):257-273 ISSN: 0976-8610 CODEN (USA): AASRFC The impact of geologic setting on the groundwater occurrence
More informationFADELE S.I, JATAU B.S AND PATRICK N.O Nasarawa State University, Keffi, Nigeria
(IJERA) ISSN: 22489622 www.ijera.com Vol. 2, Issue 5, September October 2012, pp.11431153 Geophysical Engineering Investigation Around Makiyaye Village, Shika Area Within The Basement Complex Of NorthWestern
More informationProf. Stephen A. Nelson EENS 111. Groundwater
Page 1 of 8 Prof. Stephen A. Nelson EENS 111 Tulane University Physical Geology This page last updated on 20-Oct-2003 is water that exists in the pore spaces and fractures in rock and sediment beneath
More informationElectrical Resistivity Investigation for Ground Water in Parts of Pegi, Federal Capital Territory, Nigeria
IOSR Journal of Applied Geology and Geophysics (IOSR-JAGG) e-issn: 2321 0990, p-issn: 2321 0982.Volume 2, Issue 6 Ver. I (Nov-Dec. 2014), PP 27-32 Electrical Resistivity Investigation for Ground Water
More informationHamed Aber 1 : Islamic Azad University, Science and Research branch, Tehran, Iran. Mir Sattar Meshin chi asl 2 :
Present a Proper Pattern for Choose Best Electrode Array Based on Geological Structure Investigating in Geoelectrical Tomography, in order to Get the Highest Resolution Image of the Subsurface Hamed Aber
More information2D Resistivity Imaging Investigation of Solid Waste Landfill Sites in Ikhueniro Municipality, Ikpoba Okha Local Government Area,Edo State, Nigeria.
2D Resistivity Imaging Investigation of Solid Waste Landfill Sites in Ikhueniro Municipality, Ikpoba Okha Local Government Area,Edo State, Nigeria. Iyoha. A, Akhirevbulu O.E, Amadasun C.V.O and Evboumwan
More informationGeoelectric Investigation for Groundwater Prospects in Ejeme-Aniogor and Environs, Aniocha- South Local Government Area, Delta State, Nigeria
JASEM ISSN 1119-8362 All rights reserved Full-text Available Online at www.ajol.infoand www.bioline.org.br/ja J. Appl. Sci. Environ. Manage. June 2017 Vol. 21 (4) 682-690 Geoelectric Investigation for
More informationGSJ: Volume 6, Issue 4, April 2018, Online: ISSN
GSJ: Volume 6, Issue 4, APRIL 2018 252 GSJ: Volume 6, Issue 4, April 2018, Online: ISSN 2320-9186 VERTICAL ELECTRICAL SOUNDING INVESTIGATION FOR GROUNDWATER DEVELOPMENT IN A CRYSTALLINE BASEMENT COMPLEX
More information